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The Phoenix is ‘a little stream which issues from the rocks of the west gate, whose bed is of a ruddy-brown colour, owing no doubt to its being impregnated with oxide of iron’ (Grundy, p. 284). It now joins the Spercheius rather more than half a mile below the point where that stream receives the Asopus. It is almost exactly fifteen stades from the Middle Gate and principal hot-springs at Thermopylae.

δέδμηται. The word implies an artificially constructed road, probably as now on a causeway (cf. ii. 124. 3 n.), contrasted with ὁδὸς τετμημένη (iv. 136. 2 n.).

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